Rock Identifier
White quartzite pebble (Quartzite; predominantly microcrystalline quartz (SiO₂)) — metamorphic
metamorphic

White quartzite pebble

Quartzite; predominantly microcrystalline quartz (SiO₂)

AI-generated identification · may be incorrect

Hardness about 7 Mohs; white to light gray, vitreous to sugary luster, compact granular texture, and no obvious cleavage. The rounded shape and smooth surface indicate natural water abrasion or tumbling.

Identified More metamorphic
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Physical properties

Hardness about 7 Mohs; white to light gray, vitreous to sugary luster, compact granular texture, and no obvious cleavage. The rounded shape and smooth surface indicate natural water abrasion or tumbling.

Formation & geological history

Quartzite forms when quartz-rich sandstone is recrystallized under heat and pressure, commonly during mountain-building; its exact geological age cannot be determined from the photograph. It commonly occurs in metamorphic belts and as durable stream or beach pebbles.

Uses & applications

Used as aggregate, road stone, landscaping material, decorative stone, and occasionally as a lapidary or jewelry material. This small rounded specimen has little commercial value.

Geological facts

Quartzite is generally harder and more resistant to weathering than its sandstone precursor. It can resemble white marble, but quartzite typically scratches glass while marble does not.

Field identification & locations

Field identification: test whether it scratches glass, look for a sugary quartz texture, and check that dilute acid produces no fizz; marble may fizz weakly. Common sources include mountain streams and glacial deposits worldwide.